• 한국물환경학회지
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• 제36권5호
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• pp.385-391
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• 2020

Soil loss is a serious problem frequently caused by local torrential rainfalls due to climate change. In particular, soil loss is occurring in agricultural areas rather than urban areas, and many pollutants are introduced into rivers, causing environmental problems. To reduce soil loss, the Ministry of Environment has designated and managed non-point source management areas. The Jaun-district in Hongcheon-gun, which was designed as a non-point pollution source management area in Gangwon-do, is located in the upper stream of Soyang Lake. Most of the agricultural fields are composed of highland agriculture fields. The highland agricultural fields in the Jaun-district are also composed of large-scale farming areas, and the ditches located near the agricultural fields have been illegally used for farmland. Therefore, the local government in Hongcheon-gun is conducting a project to restore the ditches occupied by agricultural fields. However, an analysis of the amount of soil loss that can be reduced by the restoration of the ditches has not been conducted yet. Thus, the purpose of this study was to analyze the effect of reducing the soil loss from the restoration of the ditches used as agricultural fields in the Jaun-district. The SATEEC L Module was used to analyze the reduction in soil loss by ditch restoration. The SATEEC L Module was constructed to estimate the LS factor using Moore and Burch's method after calculating the slope length using the digital elevation model and the maximum allowable slope length. The LS factor and the USLE formula were used to estimate the amount of soil loss that could be reduced by ditch restoration. The analysis showed that the ditch restoration could reduce about 16.6% of the soil loss in the Jaun-district. The results of this study will contribute to the study of methods to reduce soil loss in non-point pollution management areas.

• 한국환경복원기술학회지
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• 제4권1호
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• pp.16-23
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• 2001

This study was conducted to analyse the relation between physical characteristics of soil surface and wild plants occurrence. Lots of natural occurrence on loamy soil and a little of natural occurrence on perlite. Those were used to observe the wild plants occurrence through the duration. Natural occurrence of wild plants were observed on uniform sand, perlite, loamy soil and 2cms loamy soil layer above the perlite. Uniform sand was compared with different height of drain ditch. The results of analysis were as followed. 1. Wild plants germinated on the uniform perlite layer, they did not grow larger. Because water in large pores of perlite surface drained rapidly and evaporated easily, therefore surface remained low moisture contents. 2. A lot of weed grew on 2cms loamy layer on perlite which stratified above the perlite layer. Because perlite had plenty of soil moisture and soil moisture moved easily from perlite to loamy soil layer. 3. Uniform loamy soil had similar occurrence on the uniform perlite. It was nearly same at surface moisture distribution but lower than layered loamy soil on perlite, and the vertical distributions at soil moisture was totally lower than 2cms loamy soil layer on perlite. 4. Wild plants were grew on uniform sand on different height of drain ditch. In this case, much more wild plants were grew on which had more higher drainage ditch. The number of wild plants occurred when it was affected by soil surface moisture, drain ditch and natural occurrence of wild plants. This could be controlled by layered soil at surface moisture. Therefore weed occurrence can control in planting ground, where soil layer would not be disturbed.

• 한국환경복원기술학회지
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• 제2권3호
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• pp.83-92
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• 1999

To investigate the influence of forest road characteristics and site conditions on the stability of forest-road in granite area, four forest roads had been selected in Kyongbuk regions. The total of 13 road characteristic variables were evaluated by the discriminant analysis. The factors influencing the stability of forest road were bed rock, slope length, coverage, hardness, side-ditch erosion and road width. But aspect and soil texture were not significant for the stability in this area. In the correlation between forest environment and road structure, hardness and bed rock was highly significant in stability group, and coverage and side-ditch erosion was highly significant in instability group. 75 of 175 segments were instable whereas the others were stable. The centroids value by discriminant function in the stability and instability were estimated to 3.0585 and -1.9116, respectively. The stability criterion of forest road was discriminated from the centroids value of the each group. The main factors contributing the stability of forest road were significant in order of side-ditch erosion, coverage, soil texture, elevation, gradient, slope length and construction year. The prediction rate of discriminant function for stability evaluation of forest road was as high as 97.44%. In conclusion, the forest road structure factors such as length, coverage and slope gradient were controlled by construction techniques. If the factors like those should be considered in design, construction and forest road management, the stability of forest road may increase more. And also, it is necessary to take slope protection measures like small terraces and retaining walls for stability of cut slope.

• 한국농공학회논문집
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• 제66권2호
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• pp.53-62
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• 2024

This study assessed the efficiency of reducing soil erosion and suspended sediment through the restoration of alpine unauthorized and illegally cultivated fields, using the SWAT (Soil and Water Assessment Tool) model in the Mandae District. The results showed that in Scenario 5, which involved restoring unauthorized and illegal fields within forests, along rivers (banks), and in ditch areas were restored to their original land categories, achieved the highest efficiency in reducing average annual soil erosion and suspended sediment, with reductions of 8.1% and 4.5%, respectively. In particular, it was confirmed that the restoration of unauthorized and illegal fields within forested areas has a significant impact. This demonstrated that the restoration of unauthorized and illegal agricultural fields can substantially reduce the soil erosion and suspended sediment attributable to non-point source pollution. Our findings highlight the importance of managing these unauthorized and illegal agricultural activities in developing sustainable strategies within non-point source pollution management areas. This study is expected to provide important basic data to effectively establish water quality improvement strategies in the region of non-point source pollution management.

• 헤리티지:역사와 과학
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• 제51권3호
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• pp.72-87
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• 2018

본 연구는 월지의 서측 호안 일대에 존재했던 출수구(出水口)와 구거(溝渠)를 재조명하고, 서측 호안의 출수시설이 월지의 역사적 배수체계와 연관되었을 가능성에 주목하고 있다. 세부적으로는 출수구의 위치와 형태, 월지 북서측 구거와 서측 호안 출수구의 관계성, 서측 호안 출수시설의 조성시기와 성격을 중점적으로 고찰하였다. 1975년 발굴조사로 확인된 서측 호안의 출수구는 1922년 실측도면에 기록된 수낙구(水落口)와 동일시설로 판단된다. 따라서 1920년대 이전부터 월지의 서측 호안에는 별도의 출수시설이 존재했을 가능성이 높다. 서측 호안 출수구는 장방형 석재를 가공한 시설이며, 수위조절을 위한 4개의 배수공(排水孔)이 설치되어 있었다. 배수공을 통한 출수방식은 월지 북측 호안에서 조사된 출수시설과 동일하다. 1913년 제작된 지적도에서는 월지의 북서측 외곽으로 구거가 확인된다. 구거와 출수구는 근거리에 위치하며, 동일한 축선을 형성하고 있었다. 따라서 구거와 출수구는 월지의 배수체계와 연관된 유기적 시설로 판단된다. 특히 월지 북서측 구거는 서측 호안 출수시설의 조성시기를 1910년대 이전으로 소급할 수 있는 단초다. 출수구의 배수공을 통해 유입된 물은 구거를 통해 월지의 북서측 일대로 배출되었다. 서측 호안 출수시설의 조성시기와 성격은 두 가지 측면에서 해석된다. 첫 번째는 월지가 농업용 저수지로 기록되었다는 점, 월지의 북서측 일대가 농경지로 이용되었다는 점에 근거한 '조선시대의 농업용 관개시설'이다. 두 번째는 출수구가 월지의 수제선(水際線)을 형성하는 하층 호안석축에 설치되었다는 점, 최상단 배수공의 높이가 월지의 만수위(滿水位)와 유사하다는 점에 근거한 '월지 조영 당시의 수위조절용 출수시설'이다. 관련 근거와 정황을 고려하면 후자의 가능성이 더욱 높다고 판단된다.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2018년도 학술발표회
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• pp.244-244
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• 2018

전 세계적인 기후변화로 인한 기상이변 현상으로 국지성 호우가 빈번하게 발생하는 시점에 강우로 인한 토양유실 문제가 심각하게 대두되고 있다. 특히 토양유실은 도시지역보단 농업지역에서 다량 발생되고 있어 많은 영양염류가 하천으로 유입되 환경문제가 빈번히 발생되고 있다. 이러한 토양유실문제를 저감시키기 위해서 환경부에서는 비점오염원관리지역을 지정하여 관리하고 있다. 강원도 내 비점오염원관리지역으로 선정된 홍천군 자운지구는 소양호 상류에 위치한 지역으로 대부분의 농경지가 고랭지밭으로 구성되어 있다. 홍천군 자운지구 내 고랭지밭은 대규모 농업단지로 구성되어 있어 지역 내 위치한 구거가 무단으로 점용되어 농경지로 활용되는 문제점이 발생하고 있다. 이에 홍천군에서는 농경지로 점용된 구거를 복원하는 사업을 진행하고 있지만 길제 구거 복원으로 저감되는 토양유실량에 대한 분석은 수행되지 않고 있다. 따라서 본 연구에서는 비점오염원관리지역으로 지정된 홍천군 자운지구의 지적 상 농경지로 이용되고 있는 구거를 복원할 경우 발생되는 토양유실저감효과를 분석했다. 구거복원에 따른 토양유실저감효과를 분석하기 위해 사용된 모형은 SATEEC L Module이다. SATEEC L Module은 수치표고모형과 최대 허용 경사장을 이용하여 경사장을 산정한 후 Moore and Burch의 방법을 이용하여 LS factor를 산정하도록 구성되어 있다. 해당 Module을 사용하여 산정된 LS factor와 USLE 공식을 적용하여 구거 복원 시 저감되는 토양유실량을 분석했다. 분석결과 점용된 구거를 복원하면 자운지구 내 발생되는 토양유실량을 약 16.6%를 저감할 수 있는 것으로 분석되었다. 본 연구를 통해 분석된 결과는 비점오염원관리지역의 토양유실을 저감할 수 있는 방법연구에 기여할 것으로 판단된다.